Measurement of radium concentration in water with Mn-coated beads at the Sudbury Neutrino Observatory
We describe a method to measure the concentration of 224 Ra and 226 Ra in the heavy water target used to detect solar neutrinos at the Sudbury Neutrino Observatory and in the surrounding light water shielding. A water volume of 50– 400 m 3 from the detector is passed through columns which contain be...
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Published in: | Nuclear instruments & methods in physics research. Section A, Accelerators, spectrometers, detectors and associated equipment Vol. 501; no. 2; pp. 399 - 417 |
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Main Authors: | , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , |
Format: | Journal Article |
Language: | English |
Published: |
Elsevier B.V
01-04-2003
|
Subjects: | |
Online Access: | Get full text |
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Summary: | We describe a method to measure the concentration of
224
Ra
and
226
Ra
in the heavy water target used to detect solar neutrinos at the Sudbury Neutrino Observatory and in the surrounding light water shielding. A water volume of 50–
400
m
3
from the detector is passed through columns which contain beads coated with a compound of manganese oxide onto which the Ra dissolved in the water is adsorbed. The columns are removed, dried, and mounted below an electrostatic chamber into which the Rn from the decay of trapped Ra is continuously flowed by a stream of N
2 gas. The subsequent decay of Rn gives charged Po ions which are swept by the electric field onto a solid-state α counter. The content of Ra in the water is inferred from the measured decay rates of
212
Po
,
214
Po
,
216
Po
, and
218
Po
. The Ra extraction efficiency is >95%, the counting efficiency is 24% for
214
Po
and 6% for
216
Po
, and the method can detect a few atoms of
224
Ra
per m
3 and a few tens of thousands of atoms of
226
Ra
per m
3. Converted to equivalent equilibrium values of the topmost elements of the natural radioactive chains, the detection limit in a single assay is a few times
10
−16
g
Th or U/cm
3. The results of some typical assays are presented and the contributions to the systematic error are discussed. |
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ISSN: | 0168-9002 1872-9576 |
DOI: | 10.1016/S0168-9002(03)00616-8 |